Groundwater sapping as the cause of irreversible desertification of Hunshandake Sandy Lands, Inner M...
Groundwater sapping as the cause of irreversible desertification of Hunshandake Sandy Lands, Inner Mongolia, northern China
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Publisher
United States: National Academy of Sciences
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Language
English
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Publisher
United States: National Academy of Sciences
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Contents
In the middle-to-late Holocene, Earth’s monsoonal regions experienced catastrophic precipitation decreases that produced green to desert state shifts. Resulting hydrologic regime change negatively impacted water availability and Neolithic cultures. Whereas mid-Holocene drying is commonly attributed to slow insolation reduction and subsequent nonlin...
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Full title
Groundwater sapping as the cause of irreversible desertification of Hunshandake Sandy Lands, Inner Mongolia, northern China
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Record Identifier
TN_cdi_proquest_miscellaneous_1652408456
Permalink
https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_miscellaneous_1652408456
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ISSN
0027-8424
E-ISSN
1091-6490
DOI
10.1073/pnas.1418090112